相对渗透率
毛细管压力
流离失所(心理学)
润湿
接触角
同步加速器
曲率
饱和(图论)
毛细管作用
水文地质学
磁导率
矿物学
土壤孔隙空间特征
材料科学
地质学
多孔介质
机械
岩土工程
多孔性
光学
几何学
复合材料
化学
物理
心理学
生物化学
数学
组合数学
膜
心理治疗师
作者
Sajjad Foroughi,Branko Bijeljic,Martin J. Blunt
标识
DOI:10.1007/s11242-021-01609-y
摘要
Abstract We predict waterflood displacement on a pore-by-pore basis using pore network modelling. The pore structure is captured by a high-resolution image. We then use an energy balance applied to images of the displacement to assign an average contact angle, and then modify the local pore-scale contact angles in the model about this mean to match the observed displacement sequence. Two waterflooding experiments on oil-wet rocks are analysed where the displacement sequence was imaged using time-resolved synchrotron imaging. In both cases the capillary pressure in the model matches the experimentally obtained values derived from the measured interfacial curvature. We then predict relative permeability for the full saturation range. Using the optimised contact angles distributed randomly in space has little effect on the predicted capillary pressures and relative permeabilities, indicating that spatial correlation in wettability is not significant in these oil-wet samples. The calibrated model can be used to predict properties outside the range of conditions considered in the experiment.
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